Fe2+-Mg2+ partition between coexisting cordierite and garnet ? a discussion of the experimental data
- 1 January 1973
- journal article
- research article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 40 (3) , 253-258
- https://doi.org/10.1007/bf00373789
Abstract
No abstract availableKeywords
This publication has 5 references indexed in Scilit:
- Experimental study of the stability of cordierite and garnet in pelitic compositions at high pressures and temperaturesContributions to Mineralogy and Petrology, 1973
- Experimental study of the stability of cordierite and garnet in pelitic compositions at high pressures and temperaturesContributions to Mineralogy and Petrology, 1972
- Experimental study of the stability of cordierite and garnet in pelitic compositions at high pressures and temperaturesContributions to Mineralogy and Petrology, 1971
- The reaction 3 cordierite = 2 garnet + 4 sillimanite + 5 quartz as a geological thermometer in the Opinicon Lake region, OntarioContributions to Mineralogy and Petrology, 1971
- Staurolite Stability in a Part of the System Fe-Al-Si-O-HJournal of Petrology, 1968